Sentences with phrase «in atmospheric heating»

For example, BC causes an increase in atmospheric heating, accompanied by a decrease in solar heating of the surface.
Considered either way it is a major player in atmospheric heating rates.
Together, they describe variations in atmospheric heat and moisture, and how those translate into weather patterns.
If you were to calculate a change in atmospheric heat content, that would be closer to your suggestion, and while I don't think it would look much different, it is not the same metric.
I also usually try to include the change in the Relative Humidity, (if it can be found), in my graphs as humidity plays a part in the atmospheric heat content.
Why didn't you mention the role of aerosols in atmospheric heat exchanges?
Not all at once of course, but as mentioned above, when the PDO goes positive, we can likely expect a significant change in the atmospheric heat content as heat energy is transferred from the deep oceans back into the atmosphere.
Interannual variations in the atmospheric heat budget Kevin E. Trenberth, David P. Stepaniak, and Julie M. Caron JOURNAL OF GEOPHYSICAL RESEARCH, VOL.

Not exact matches

«Clouds are one of the major feedbacks in cooling and heating the surface» of the ice, said Nate Miller, an atmospheric science graduate student at the University of Wisconsin, Madison.
The challenge may arise from the models» inability to adequately represent the atmospheric heating associated with changes in cloud populations.
«Volcanic aerosols in the stratosphere absorb infrared radiation, thereby heating up the stratosphere, and changing the wind conditions subsequently,» said Dr. Matthew Toohey, atmospheric scientist at GEOMAR Helmholtz Centre for Ocean Research Kiel.
«I knew just from basic physics that there would be a point at which heat and humidity would become intolerable, and it didn't seem that anyone had looked at that from a climate change perspective,» says Steven Sherwood, an atmospheric scientist at the University of New South Wales in Sydney, Australia.
Knowing what to look for Previous studies investigating heat wave prediction have looked for patterns in the tropics, but this research was interesting because the predictive factor is an atmospheric phenomenon that occurs in the middle latitudes, Schubert said.
Computer model finds historical patterns In order to learn that this atmospheric pattern exists in advance of heat waves, Teng and her co-authors had to look far back in the history of heat waves — from before weather records were kepIn order to learn that this atmospheric pattern exists in advance of heat waves, Teng and her co-authors had to look far back in the history of heat waves — from before weather records were kepin advance of heat waves, Teng and her co-authors had to look far back in the history of heat waves — from before weather records were kepin the history of heat waves — from before weather records were kept.
Of course, the extra heat trapped by human greenhouse gas emissions is likely to play a bigger role than raindrop friction in any atmospheric changes.
Instead of dissipating into space, the infrared radiation that is absorbed by atmospheric water vapor or carbon dioxide produces heating, which in turn makes the earths surface warmer.
«But on top of that, changes in atmospheric circulation can favor particular weather conditions associated with heat waves.»
Coumou has examined the waviness of the jet stream in previous work and has suggested that its large twists and turns, slow - moving undulations called Rossby waves, promote atmospheric «blocking» — a kind of stagnation of weather patterns that he says can exacerbate heat waves.
Francesco Panerai of Analytical Mechanical Associates Inc., a materials scientist leading a series of X-ray experiments at Berkeley Lab for NASA Ames Research Center, discusses a 3 - D visualization (shown on screens) of a heat shield material's microscopic structure in simulated spacecraft atmospheric entry conditions.
They created Ti3N4 in a cubic crystalline phase using a laser - heated diamond anvil cell, which was brought to about 740,000 times normal atmospheric pressure (74 gigapascals) and about 2,200 degrees Celsius (2,500 kelvin).
That excess tropical energy fueled rising air in a process known as convection, creating rain, releasing heat, and forming large - scale atmospheric patterns called Rossby waves.
NASA Ames Research Center (NASA ARC) in California's Silicon Valley has traditionally used extreme heat tests at its Arc Jet Complex to simulate atmospheric entry conditions.
Scientists finally confirmed this hypothesis in the 1960s when it became possible to develop adequate models of solar atmospheric heating.
Using 19 climate models, a team of researchers led by Professor Minghua Zhang of the School of Marine and Atmospheric Sciences at Stony Brook University, discovered persistent dry and warm biases of simulated climate over the region of the Southern Great Plain in the central U.S. that was caused by poor modeling of atmospheric convective systems — the vertical transport of heat and moisture in the atmosphere.
The continuation of current trends in shrub and tree expansion could further amplify this atmospheric heating by two to seven times.
Another principal investigator for the project, Laura Pan, senior scientist at the National Center for Atmospheric Research in Boulder, Colo., believes storm clusters over this area of the Pacific are likely to influence climate in new ways, especially as the warm ocean temperatures (which feed the storms and chimney) continue to heat up and atmospheric patterns continue to evolve.
Sulphur particles in the stratosphere reflect sunlight and therefore act antagonistically to atmospheric greenhouse gases like CO2, which capture the heat of the sun on Earth.
But it is a complicated picture: the effect that extra atmospheric CO2 has in these kind of experimental setups might not reflect its effects in the real world, where other factors — such as elevated heat, or changes in precipitation — come into play.
This is due to the unabated upward trends in human population growth (6), atmospheric heat content, and OA (2).
In the North Atlantic, more heat has been retained at deep levels as a result of changes to both the ocean and atmospheric circulations, which have led to the winter atmosphere extracting less heat from the ocean.
[NASA's OCO - 2 Mission in Pictures (Gallery)-RSB- The concentration of atmospheric carbon dioxide — a heat - trapping «greenhouse gas» — has risen from 280 parts per million (ppm) before the Industrial Revolution to about 400 ppm today.
The UM Rosenstiel School researchers used historical observations of cloud cover as a proxy for wind velocity in climate models to analyze the Walker circulation, the atmospheric air flow and heat distribution in the tropic Pacific region that affects patterns of tropical rainfall.
As a result of atmospheric patterns that both warmed the air and reduced cloud cover as well as increased residual heat in newly exposed ocean waters, such melting helped open the fabled Northwest Passage for the first time [see photo] this summer and presaged tough times for polar bears and other Arctic animals that rely on sea ice to survive, according to the U.S. Geological Survey.
Scientists have fingerprinted a distinctive atmospheric wave pattern high above the Northern Hemisphere that can foreshadow the emergence of summertime heat waves in the United States more than two weeks in advance.
That could allow heat from the ocean to be released into the atmosphere — causing a jump in atmospheric global warming, Trenberth says: «This could be a very important year.»
Previous studies have hypothesized that the North Pacific atmospheric ridge is caused by increased ocean surface temperatures and movement of heat in the tropical Pacific.
All that extra heat in the Pacific warms the air above, leading to more rising air than normal in that region, which affects the global atmospheric circulation.
Increasing atmospheric CO2 concentrations cause an imbalance in Earth's heat budget: more heat is retained than expelled, which in turn generates global surface warming.
the Arctic has shown a pattern of strong low - level atmospheric warming over the Arctic Ocean in autumn because of heat loss from the ocean back to the atmosphere....
Because Uranus has no internal source of heat, its atmospheric activity was thought to be driven solely by sunlight, which is now weak in the northern hemisphere.
I am excited about our results because they open a new window on very fundamental processes in brown dwarfs (atmospheric circulation, heat exchanges, and cloud formation) and, at the same time, they also explain a number of past observations that puzzled brown dwarf experts.
Therefore, the strongest motivation for the current scientific review is the need for a synoptic organization of the available knowledge on the field of interactions at different planetary systems, in parallel with a comparative analysis encompassing the inter-connection among planetary space weather aspects belonging to different disciplines (e.g. plasma variability and its effects on atmospheric heating).
Gray believes that the increased atmospheric heat — which he calls a «small warming» — is ``... likely a result of the natural alterations in global ocean currents which are driven by ocean salinity variations.»
The atmospheric greenhouse effect, an idea that authors trace back to the traditional works of Fourier 1824, Tyndall 1861, and Arrhenius 1896, and which is still supported in global climatology, essentially describes a fictitious mechanism, in which a planetary atmosphere acts as a heat pump driven by an environment that is radiatively interacting with but radiatively equilibrated to the atmospheric system.
For example, in Earth atmospheric circulation (such as Hadley cells) transport heat between the warmer equatorial regions to the cool polar regions and this circulation pattern not only determines the temperature distribution, but also sets which regions on Earth are dry or rainy and how clouds form over the planet.
But the burning of oil, coal, and gas also caused most of the historical increase in atmospheric levels of heat - trapping greenhouse gases.
For as much as atmospheric temperatures are rising, the amount of energy being absorbed by the planet is even more striking when one looks into the deep oceans and the change in the global heat content (Figure 4).
Changes in Hadley circulation affects convection and thus atmospheric moisture content and cloud cover which may in turn affect net solar heating as well as the transfer of heat from Earth to space.
Polar amplification, in which temperatures at the poles rise more rapidly than temperatures at the equator (due to factors like the global atmospheric and oceanic circulation of heat from the equator to the poles), plays a major role in the rate of ice sheet retreat.
Using atmospheric data from the last 35 years, study author Daniel Horton, a Stanford University postdoc, and his colleagues found that persistent areas of high pressure in certain places were linked with extreme heat waves in Europe, western Asia and eastern North America.
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